9 research outputs found
Honey Yield Forecast Using Radial Basis Functions
Honey yields are difficult to predict and have been usually
associated with weather conditions. Although some specific meteorological
variables have been associated with honey yields, the reported relationships
concern a specific geographical region of the globe for a given
time frame and cannot be used for different regions, where climate may
behave differently. In this study, Radial Basis Function (RBF) interpolation
models were used to explore the relationships between weather variables
and honey yields. RBF interpolation models can produce excellent
interpolants, even for poorly distributed data points, capable of mimicking
well unknown responses providing reliable surrogates that can
be used either for prediction or to extract relationships between variables.
The selection of the predictors is of the utmost importance and an
automated forward-backward variable screening procedure was tailored
for selecting variables with good predicting ability. Honey forecasts for
Andalusia, the first Spanish autonomous community in honey production,
were obtained using RBF models considering subsets of variables
calculated by the variable screening procedure
Scaled distribution mapping: a bias correction method that preserves raw climate model projected changes
Commonly used bias correction methods such as quantile
mapping (QM) assume the function of error correction values between modeled
and observed distributions are stationary or time invariant. This article
finds that this function of the error correction values cannot be assumed to
be stationary. As a result, QM lacks justification to inflate/deflate
various moments of the climate change signal. Previous adaptations of QM,
most notably quantile delta mapping (QDM), have been developed that do not
rely on this assumption of stationarity. Here, we outline a methodology
called scaled distribution mapping (SDM), which is conceptually similar to
QDM, but more explicitly accounts for the frequency of rain days and the
likelihood of individual events. The SDM method is found to outperform QM,
QDM, and detrended QM in its ability to better preserve raw climate model
projected changes to meteorological variables such as temperature and
precipitation
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From California’s Extreme Drought to Major Flooding: Evaluating and Synthesizing Experimental Seasonal and Subseasonal Forecasts of Landfalling Atmospheric Rivers and Extreme Precipitation during Winter 2022/23
California experienced a historic run of nine consecutive landfalling atmospheric rivers (ARs) in three weeks’ time during winter 2022/23. Following three years of drought from 2020 to 2022, intense landfalling ARs across California in December 2022–January 2023 were responsible for bringing reservoirs back to historical averages and producing damaging floods and debris flows. In recent years, the Center for Western Weather and Water Extremes and collaborating institutions have developed and routinely provided to end users peer-reviewed experimental seasonal (1–6 month lead time) and subseasonal (2–6 week lead time) prediction tools for western U.S. ARs, circulation regimes, and precipitation. Here, we evaluate the performance of experimental seasonal precipitation forecasts for winter 2022/23, along with experimental subseasonal AR activity and circulation forecasts during the December 2022 regime shift from dry conditions to persistent troughing and record AR-driven wetness over the western United States. Experimental seasonal precipitation forecasts were too dry across Southern California (likely due to their overreliance on La Niña), and the observed above-normal precipitation across Northern and Central California was underpredicted. However, experimental subseasonal forecasts skillfully captured the regime shift from dry to wet conditions in late December 2022 at 2–3 week lead time. During this time, an active MJO shift from phases 4 and 5 to 6 and 7 occurred, which historically tilts the odds toward increased AR activity over California. New experimental seasonal and subseasonal synthesis forecast products, designed to aggregate information across institutions and methods, are introduced in the context of this historic winter to provide situational awareness guidance to western U.S. water managers
Scaled distribution mapping: a bias correction method that preserves raw climate model projected changes
Commonly used bias correction methods such as quantile mapping (QM) assume the function of error correction values between modeled and observed distributions are stationary or time invariant. This article finds that this function of the error correction values cannot be assumed to be stationary. As a result, QM lacks justification to inflate/deflate various moments of the climate change signal. Previous adaptations of QM, most notably quantile delta mapping (QDM), have been developed that do not rely on this assumption of stationarity. Here, we outline a methodology called scaled distribution mapping (SDM), which is conceptually similar to QDM, but more explicitly accounts for the frequency of rain days and the likelihood of individual events. The SDM method is found to outperform QM, QDM, and detrended QM in its ability to better preserve raw climate model projected changes to meteorological variables such as temperature and precipitation.Austrian Federal Ministry of Agriculture, Forestry, Environment and Water Management [OKS15]; Austrian Klima- und Energiefonds through the Austrian Climate Research Program (ACRP) [B368584, B464795]open access journalThis item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at [email protected]
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From California’s Extreme Drought to Major Flooding Evaluating and Synthesizing: Experimental Seasonal and Subseasonal Forecasts of Landfalling Atmospheric Rivers and Extreme Precipitation during Winter 2022/23
California experienced a historic run of nine consecutive landfalling atmospheric rivers (ARs) in three weeks’ time during winter 2022/23. Following three years of drought from 2020 to 2022, intense landfalling ARs across California in December 2022–January 2023 were responsible for bringing reservoirs back to historical averages and producing damaging floods and debris flows. In recent years, the Center for Western Weather and Water Extremes and collaborating institu-; tions have developed and routinely provided to end users peer-reviewed experimental seasonal (1–6 month lead time) and subseasonal (2–6 week lead time) prediction tools for western U.S. ARs, circulation regimes, and precipitation. Here, we evaluate the performance of experimental seasonal precipitation forecasts for winter 2022/23, along with experimental subseasonal AR activity and circulation forecasts during the December 2022 regime shift from dry conditions to persistent troughing and record AR-driven wetness over the western United States. Experimental seasonal precipitation forecasts were too dry across Southern California (likely due to their over-reliance on La Niña), and the observed above-normal precipitation across Northern and Central California was underpredicted. However, experimental subseasonal forecasts skillfully captured the regime shift from dry to wet conditions in late December 2022 at 2–3 week lead time. During this time, an active MJO shift from phases 4 and 5 to 6 and 7 occurred, which historically tilts the odds toward increased AR activity over California. New experimental seasonal and subseasonal synthesis forecast products, designed to aggregate information across institutions and methods, are introduced in the context of this historic winter to provide situational awareness guidance to western U.S. water managers. © 2024 American Meteorological Society. This published article is licensed under the terms of the default AMS reuse license. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy (www.ametsoc.org/PUBSReuseLicenses).6 month embargo; first published 08 January 2024This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at [email protected]